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Development of new seismic hazard maps of Indonesia 2017
Irsyam M.a, Hendriyawanb, Natawijaya D.H.c, Daryono M.R.c, Widiyantoro S.b, Asrurifak M.b, Meilano I.b, Triyoso W.b, Hidayati S.d, Rudiyanto A.e, Sabaruddin A.f, Faisal L.f
a Indonesian Society for Geotechnical Engineering, Indonesia
b Faculty of Civil and Environmental Engineering, Institute of Technology Bandung, Indonesia
c Research Center for Geotechnology, Indonesian Institute of Science, Indonesia
d Center of Volcanology and Geological Hazard Mitigation, Geological Agency, Indonesia
e Meteorological Climatological and Geophysical Agency, Indonesia
f Ministry of Public Works, Indonesia
[vc_row][vc_column][vc_row_inner][vc_column_inner][vc_separator css=”.vc_custom_1624529070653{padding-top: 30px !important;padding-bottom: 30px !important;}”][/vc_column_inner][/vc_row_inner][vc_row_inner layout=”boxed”][vc_column_inner width=”3/4″ css=”.vc_custom_1624695412187{border-right-width: 1px !important;border-right-color: #dddddd !important;border-right-style: solid !important;border-radius: 1px !important;}”][vc_empty_space][megatron_heading title=”Abstract” size=”size-sm” text_align=”text-left”][vc_column_text]© 2017 19th ICSMGE Secretariat. All rights reserved.This paper presents the progress in developing Indonesia seismic hazard maps. The revision of seismic hazard maps has been developed based upon updated: seismotectonic data, fault models, and GMPEs. Important information is considered for updating seismic hazard maps such as significant results of recent active-fault studies utilizing trenching, carbon dating, epicenter relocation, strain analysis (GPS) as well as availability of basic data including the SRTM-30, IFSAR, LiDAr and other data that is just recently available. The new information was gathered in order to obtain more accurate tectonic model and their seismic parameters, such as maximum magnitudes and slip-rates. Based on the latest researches and investigations, revised seismotectonic models for Indonesia were developed and used in developing new seismic hazard maps. Finally, probabilistic and deterministic analyses were then performed in order to develop new seismic hazard maps 2017.[/vc_column_text][vc_empty_space][vc_separator css=”.vc_custom_1624528584150{padding-top: 25px !important;padding-bottom: 25px !important;}”][vc_empty_space][megatron_heading title=”Author keywords” size=”size-sm” text_align=”text-left”][vc_column_text]Deterministic analysis,Maximum magnitudes,Peak ground acceleration,Seismic hazard maps,Seismic hazards,Seismic parameters,Seismotectonics,Tectonic models[/vc_column_text][vc_empty_space][vc_separator css=”.vc_custom_1624528584150{padding-top: 25px !important;padding-bottom: 25px !important;}”][vc_empty_space][megatron_heading title=”Indexed keywords” size=”size-sm” text_align=”text-left”][vc_column_text]New seismotectonic model,Peak ground acceleration,Probabilistic and deterministic seismic hazards[/vc_column_text][vc_empty_space][vc_separator css=”.vc_custom_1624528584150{padding-top: 25px !important;padding-bottom: 25px !important;}”][vc_empty_space][megatron_heading title=”Funding details” size=”size-sm” text_align=”text-left”][vc_column_text][/vc_column_text][vc_empty_space][vc_separator css=”.vc_custom_1624528584150{padding-top: 25px !important;padding-bottom: 25px !important;}”][vc_empty_space][megatron_heading title=”DOI” size=”size-sm” text_align=”text-left”][vc_column_text][/vc_column_text][/vc_column_inner][vc_column_inner width=”1/4″][vc_column_text]Widget Plumx[/vc_column_text][/vc_column_inner][/vc_row_inner][/vc_column][/vc_row][vc_row][vc_column][vc_separator css=”.vc_custom_1624528584150{padding-top: 25px !important;padding-bottom: 25px !important;}”][/vc_column][/vc_row]